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Mount Coleman 山峰

3,135 米海拔
775 米相对高度
加拿大位置图Mount Coleman

示意图,边界据 Natural Earth,不作为划界依据。

资料

所在国家 / 地区
加拿大
坐标
北纬 52.12°,西经 116.92°
所属山脉
Cloister Mountains
所在保护区
班夫国家公园

百科(英文)

这个词条没有中文维基百科条目,下面是英文维基百科的原文。

Mount Coleman is a 3,135-metre (10,285 ft) mountain summit located in the upper North Saskatchewan River valley in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Cirrus Mountain, 4.46 km (2.77 mi) to the north. Mount Coleman is situated along the east side the Icefields Parkway midway between Saskatchewan Crossing and Sunwapta Pass.

History

Mount Coleman was named in 1898 after Arthur P. Coleman (1852-1939), a Canadian geologist and among the first white men to explore the area that is now Jasper National Park.

Geology

Like other mountains in Banff Park, Mount Coleman is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.

Climate

Based on the Köppen climate classification, Mount Coleman is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Coleman drains into tributaries of the North Saskatchewan River.

以上摘自英文维基百科「Mount Coleman (Alberta)」(去掉了表格、图片、参考文献和外部链接),按 CC BY-SA 4.0 使用。

Mount Coleman
图:Neil · CC BY 2.0 · 来自 Wikimedia Commons

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